Neptunian sills at Rocca Busambra, a fragment of the Trapanese/Saccense Domain in western Sicily, host themost abundant ammonite and gastropod fauna which has ever been recorded from the Jurassic of the westernTethys. The fauna is dominated by parautochthonous organisms which were swept into the sills by gentletransport. Ammonites are characterized by perfect preservation and small size, a feature which is due to thepredominance of microconchs but also of stunting. The most complete sill is 0.7 m thick and could be separatedinto 17 levels which range in age from the early Toarcian into the late Kimmeridgian, thus representing the mostextreme case of palaeontologically and depositionally documented stratigraphic condensation in Earth history.The unique feature of the Rocca Busambra sills is due to the interaction of three processes: extreme stratigraphiccondensation on the sea floor, weak tectonic fracturing of the host rock and repeated reopening on top of alreadyexisting sills. Contrasting percentages of gastropods in individual levels reflect sea-level oscillations whichcorrespond to long known low- and highstands during the Jurassic of the western Tethys. Comparisons withother ammonite-bearing sill faunas reveal several similarities, but represent only short-timed phases of tectonicpulses and deposition.
